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20篇 您的检索式:作者名="PENG Fubing"
    题名 作者 年代 出处 被引量
1Diffusion behavior of benzene/cyclohexane molecules in poly(vinyl alcohol)-graphite hybrid membranes by molecular dynamics simulation显示文摘Pan Fusheng Peng Fubing Jiang Zhongyi 2007Chemical EngineeringScinece2007,62,3:1
2Novel ploy(vinyl alcohol)/carbon nanotube hybrid membranes for pervaporation separation of benzene/cyclohexane mixtures显示文摘Fubing Peng Changlai Hu Zhongyi Jiang 2007Journal of Membrane Science2007,,1:1
3Synthesis and characterization of novel swelling tunable olignmeric poly( styrene-co-acrylamide) modified clays显示文摘Chen ruyi Peng Fubing Su Shengpei 2008J Appl Polym Sci2008,108,4:1
4Removing benzene from aqueous solution using CMS-filled PDMS pervaporation membranes显示文摘Peng Fubing Jiang Zhongyi Hu Changla 2006Separation and Purification Technology2006,48,3:1
5Transport, structural and in- terracial properties of poly (vinyl alcohol)-polysulfone composite nanofiltration membranes显示文摘Peng Fubing Huang Xiaofei 2010Joumal''of Mem-brane Science2010,353,:1
6Organic-inorganic hybrid membranes with simultaneously enhanced flux and selectivity 显示文摘Peng Fubing Lu Lianyu Sun Honglei 2007Industrial and Engineering Chemistry Research2007,46,8:1
7Novel nanocomposite pervaporation membranes composed of poly(vinyl alcohol) and chitosan-wrapped carbon nanotube显示文摘Fubing Peng Fusheng Pan Honglei Sun Lianyu Lu Zhongyi Jiang 2007Journal of Membrane Science2007,,1:1
8Synthesis and characterization of novel swelling tunable oligomeric poly( styrene-co-acrylamide) modified clays 显示文摘Chen Ruyi Peng Fubing Su Shengpei 2008J Appl Polym Sci2008,108,4:1
9Diffusion behavior of benzene/cyclohexane molecules in poly (vinylalcohol)-graphite hybrid membranes by molecular dynamics simulation 显示文摘Pan Fusheng Peng Fubing Jiang Zhongyi 2007Chemical Engineering Science2007,62,:1
10Re- moving benzene from aqueous solution using CMS-filledPDMS pervaporation membranes 显示文摘Peng Fubing Jiang Zhongyi Hu Changlai 2006Sep Purif Technol2006,48,:1
11Synthesis and characterization of novel swelling tunable oligomeric poly (styrene-co-acrylamide) modified clays显示文摘CHEN ruyi PENG Fubing SU Shengpei 2008J Appl Polym Sci2008,108,:1
12Pervaporation Properties of PDMS Membranes for Removal of Benzene from Aqueous Solution: Experimental and Modeling 显示文摘Peng Fubing Pan Fusheng Li Duo 2005Chem EngJ2005,114,13:1
13Diffusion be-havior of benzene/cyclohexane molecules in poly (vinyl alcohol)-graphite hybrid membranes by molecular dynamics simulation 显示文摘Pan Fusheng Peng Fubing Jiang Zhongyi 2007Chemical Engineering Science2007,,62:1
14Correlations between free volume characteristics and pervaporation permeability of novel PVA-GPTMS hybrid membranes显示文摘Peng Fubing 2006Journal of Membrane Science2006,,275:1
15Analysis of annealing effect on pervaporation properties of PVA-GPT- MS hybrid membranes through PALS显示文摘Peng Fubing Lu Lianyu Sun Honglei 2006Journal of Membrane Science2006,,281:1
16Removing benzene from aqueous solution using CMS-fiUed PDMS pervaporation membranes显示文摘Peng Fubing Jiang Zhongyi Hu Changlai 2006Separation and Purification Technology2006,48,3:1
17Research on simulation evaluation of strategic projection base construction planning in ExtendSim environment 显示文摘Peng Fubing Dun E Er Cui Tenglong 2014Applied Mechanics and Ma- terials2014,641,:1
18Re- moving benzene from aqueous solution using CMS- filled PDMS pervaporation membranes显示文摘Peng Fubing Jiang Zhongyi Hu Changlai etal 2006Sep Purif Tech2006,48,:1
19Hybrid organicinorganic membrane:solving the tradeoff between permeability and selectivity显示文摘Peng Fubing Lu Lianyu Sun Honglei 2005Chem Mater2005,17,:1
20Sedimentary and tectonic evolution of the Banquan pull-apart basin and implications for late Cenozoic dextral strike-slip movement of the Tanlu Fault Zone显示文摘The Banquan Basin is a pull-apart basin with the largest scale and the most prominent structure due to dextral slip of the Tanlu Fault Zone(TLFZ) in late Cenozoic. The depositional history of the basin records the start time and evolution of the right-lateral strike-slip movement of the TLFZ. This paper studies the sedimentary and tectonic evolution of the Banquan Basin by seismic reflection exploration, borehole detection and cosmogenic nuclide chronology. We analyze the coupling relationship between the pull-apart basin and the strike-slip fault and discuss the start time and tectonic significance of the right-lateral strikeslip of the TLFZ. Our study indicates that the Banquan Basin has undergone three evolutionary stages: weak rifting during the pre-pull-apart period, strong extension during the syn-pull-apart period and subsidence during the post-pull-apart period. This implies that the TLFZ, which controls the evolution of the basin, experienced an evolutionary process of weak activity,intensified activity and migration of activity toward the central basin. The sedimentary filling of the basin has strong response to the episodic pull-apart and extension of the basin. Lying upon the basement of the basin, a thin layer of Miocene mudstone slowly accumulated due to local rifting before the strong pull-apart event. Along with the dextral slipping and pull-apart process, the basin was filled with alluvial fan facies, fluvial facies and floodplain facies strata from bottom to top. The latest tectonic movement of the TLFZ in the North China Block in late Cenozoic was dominated by episodic dextral strike-slip motion, and this deformation pattern started at 4.01±1.27 Ma. The latest tectonic deformation in North China since late Cenozoic was governed by eastward extrusion and tectonic orogenesis of the eastern margin of the Qinghai-Xizang Plateau since late Miocene. The eastward thrusting of the Liupanshan fault zone and sinistral shearing of the Qinling fault zone led to the anticlockwise rotation and pushing of secondary blocks in North China, resulting in a planar bookshelf faulting and rotation pattern. This unique deformation pattern transferred eastwards to the North China Plain at ~4.01 Ma and the process continues to the present time.This planar bookshelf rotation, accompanied with regional sinistral strike-slip movement of the ~EW-trending boundary fault zones to the north and south of the North China Block and dextral strike-slip motion of the NNE-trending boundary faults between secondary blocks, is likely to be the long-range effect of the strong extrusion of the eastern margin of the QinghaiXizang Plateau.Peng SHU Xiwei XU Shaoying FENG Baojin LIU Kang LI Paul TAPPONNIER Xiaojuan DENG Guihua CHEN Nuan XIA Hongtai XU Jingjing QIN Fubing HE Yan MA Rongzhang ZHENG 2023Science China Earth Sciences2023,66,4:0
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